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Saint Mary Road Bethal Road CR 280 Washington-Holmes County Line former SR 173 [1] CR 179: Wrights Creek Road US 90: Washington-Holmes County Line former SR 179 [1] CR 273: E.L. Kham Boulevard Washington Boulevard Orange Hill Road South Boulevard SR 77: SR 277: former SR 273 [1] CR 276: Piney Grove Road Clayton Road Alford Highway SR 277 ...
The old road from Fork of the Road eastward along the Mojave River is interrupted after 10.9 acres (4.4 ha) by private property, below the site of the old Camp Cady (on the north bank of the Mojave River, roughly 12 miles (19 km) northeast of Newberry Springs). The road is resumed at an access point from the north in Manix Wash. Under optimal ...
The city removed recycling drop boxes from its north Richland recycling station this week, saying the ongoing problem of dumped furniture and other garbage as well as homeless camping rendered it ...
Point of Rocks was a landmark along the Mojave Trail, and its successors, the Old Spanish Trail and the Mormon Road that followed the riverbed. [2] It marked a point where the Mojave River would appear above ground to run on the surface surrounded by grassland, marshes and groves of cottonwood and willow.
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Fork of the Road was the locale along the Mojave River where the junction of the Mojave Trail / Mojave Road and the Old Spanish Trail / Mormon Road was located in San Bernardino County, California. The location of Fork of the Road was on the north side of the Mojave River, 18.75 miles southwest of Bitter Spring , about 14.5 miles east of ...
Charles Street and Kanes Falls Road in Fort Ann: Fish Hill Road CR 17: 8.28 13.33 NY 149 in Hartford: Bull Hill Road NY 22 in Granville: CR 17A: 0.79 1.27 CR 17 West Granville Spur in Fort Ann: NY 22: CR 18: 7.19 11.57 US 4 in Whitehall: Brick Church Road NY 22A in Hampton: Formerly NY 273: CR 18A: 0.20 0.32 NY 22A: Poultney Road in Hampton ...
The Mojave River is an intermittent river in the eastern San Bernardino Mountains and the Mojave Desert in San Bernardino County, California, United States. Most of its flow is underground, while its surface channels remain dry most of the time, except for the headwaters and several bedrock gorges in the lower reaches.